What is Anabatic Wind?

Local winds that blow from slopes to peaks as a result of the heating of the top slopes without being affected by general pressure changes. Generally, the term is used for upward air currents, vertical movements in the formation of cumulus clouds, and valley breezes rather than anabatic winds. Anabatic winds are less common than katabatic winds, which occur through the opposite process.

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Glossary

The narrow region between 35-40 ° N and S latitudes in the Northern and Southern Hemispheres, lying between the tropical...

Considerable cloudiness refers to weather conditions where a large portion of the sky is covered with clouds, but some clear...

A low-pressure area with converging winds, rotating counterclockwise in the Northern Hemisphere and clockwise in the Southern...

A cloud of irregular appearance, composed of irregular cloud fragments.

A type of low-altitude cloud that forms in uniform layers, often covering the entire sky and producing overcast conditions.

Jet streams are strong, fast-flowing air currents in the upper levels of the atmosphere. They form when warm air masses meet...

A condition in which the stratification of the atmosphere depends on both air temperature and pressure, and where surfaces...

Bright and dark rays with changing colors and contrast in the sky. These rays become visible due to the reflection of atmospheric...

A prefix used in cloud nomenclature to describe middle-altitude clouds that form between 6,500 and 20,000 feet, such as altostratus...

The heating of the Earth by the sun causes daily changes in both the direction and speed of the wind. During the day, ground...

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